TY - JOUR
T1 - 3D Seismic Analysis Reveals the Origin of Ambiguous Erosional Features at a Major Sequence Boundary in the Eastern North Sea: near Top Oligocene
JF - Geological Society, London, Memoirs
JO - Geological Society, London, Memoirs
SP - 83
LP - 90
DO - 10.1144/GSL.MEM.2004.029.01.09
VL - 29
IS - 1
AU - Hansen, J. P. V.
AU - Clausen, O. R.
AU - Huuse, M.
Y1 - 2004/01/01
UR - https://mem.lyellcollection.org/content/29/1/83.abstract
N2 - The near top Oligocene unconformity is a major sequence boundary in the eastern North Sea Basin. It is characterized by erosional scarps below the boundary and a pronounced basinward shift in onlap above. The shift in onlap has previously been interpreted as caused by a major fall in sea level. Detailed 3D seismic analysis of a 20 by 20 km area at and basinward of the uppermost Oligocene clinoform breakpoint reveals that the erosional scarps were caused by undercutting of steep clinoforms by contour-parallel currents and resulting mass wasting whilst the lowermost onlap package consists of a contour-parallel drift deposited as the erosive currents waned. The 3D seismic analysis corroborates a recent analysis based on regional 2D seismic data, which found that the erosional scarps and the geometry of the onlap sequence were indicative of a major shift in sediment input directions and not necessarily associated with any change of sea level. The paper thus demonstrates the utility of local 3D seismic analyses as a form of 'ground truthing' regional basin analyses based on widely spaced 2D seismic grids.
ER -